Figure 1From: A long-term slow slip event from 1996 to 1997 in the Kii Channel, JapanRegional tectonic setting and location of the study area. Solid lines indicate plate boundaries. The rectangle is the region shown in Figure 2. Red dots indicate the epicenters of low-frequency earthquakes along the Nankai Trough from January 2006 to December 2010. Stars indicate the epicenters of the 1944 Tonankai and the 1946 Nankai earthquakes. Labels A to D show locations of long-term slow slip events (SSEs) along the Nankai Trough observed by GPS. A: Tokai (Suito and Ozawa 2009). B: western Shikoku (Kobayashi 2010). C: Bungo Channel (Hirose et al. 2010). D: Hyuga-nada (Yarai and Ozawa 2013).Back to article page